∂Q/∂x + ∂A/∂t = 0 ∂Q/∂x + B ∂y/∂t = 0 r = ∂y/∂t ∂Q/∂x + B r = 0 Qd - Qu = - B (Δx) r Qu = Qd + B (Δx) r Qu = 650 + 280 (25,000) (4 mm/hr / 3600 s/hr) (1 m / 1000 mm) Qu = 657.78 m3 ANSWER.
∂Q/∂x + ∂A/∂t = 0 ∂Q/∂x + B ∂y/∂t = 0 r = ∂y/∂t ∂Q/∂x + B r = 0 ra = 0.5 (ru + rd) = 6.0 Qd - Qu = - B (Δx) ra Qu = Qd + B (Δx) ra Qu = 650 + 280 (25,000) (6.0 mm/hr / 3600 s/hr) (1 m / 1000 mm) Qu = 661.67 m3 ANSWER. The second estimate is more accurate, because it is a central finite difference.
F2 = q2/(gy3) y = [q2/(gF2 ]1/3 = 3.44 m. F = v/(gy)1/2 = 0.2 v = 0.2 (gy)1/2 cr= (gy)1/2 = (9.81 × 3.44) 1/2 = 5.81 m/s v = 0.2 × 5.81 = 1.16 m/s cd = v + cr = 1.16 + 5.81 = 6.97 m/s ANSWER. cu = v - cr = 1.16 - 5.81 = -4.65 m/s ANSWER.
Peak flood Qp= 600 m3/s; baseflow Qb= 100 m3/s; So = 0.0007; Ap = 350 m2; Tp = 85 m; β = 1.65; Δx = 9.8 km = 9,800 m; Δt = 1 hour = 3,600 s.
The mean velocity Vp= Qp/Ap = 600/350 = 1.714 m/s. The wave celerity is: The flow per unit width qo = Qp/Tp = 600/85 = 7.059 m2/s. The Courant number C = c Δt/Δx = 2.828 m/s × 3600 s / 9,800 m = 1.039 The cell Reynolds number D = qo/(Soc Δx) = (7.059) / (0.0007 × 2.828 × 9,800) = 0.364 The routing coefficients are: C0 = 0.168; C1 = 0.697; and C2 = 0.135. The routing calculations are shown below.
The peak outflow is 581.351 and it occurs at time 11 hr. The wave has diffused from a peak of 600 to 581, and has translated from t = 10 hr to t = 11 hr. ANSWER.
|